Download Pdf File
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Programme Monday, March 24
23rd LAK, 2014, Heidelberg Programme 13 Programme Monday, March 24 INF 252, Hörsäle Chemie 18:00– CONFERENCE DESK OPENING 21:00 18:00– ICEBREAKER PARTY 22:00 * Sponsored by DFG travel grants 14 Programme 23rd LAK, 2014, Heidelberg Tuesday I, March 25 INF 252, Hörsaal Ost INF 252, Hörsaal West 09:30 Welcome Christina Ifrim and Wolfgang Stinnesbeck DAAD-Fördermöglichkeiten für Geowissenschaftler aus/nach Lateinamerika Sybilla Tinnap, DAAD, Bonn Talk 141: Funding Opportunities for Scientific and Technological Cooperation: The Role of the Project Management Agency European and International Cooperation International Bureau of the Bmbf Inge Lamberz de Bayas, Internationales Büro, Bundesministerium für Bildung und Forschung, Bonn International Cooperation in DFG-Programmes – Earth Sciences in Latin America Dietrich Halm, DFG, Bonn 11:00 COFFEE BREAK and POSTER SESSION Session 1: The southernmost dinosurs in Latin Session 2: Water America and their environment Chair: Heinrich Adolf Horn Chair: Marcelo Leppe 11:20 Talk 205: Late Cretaceous Terrestrial Biota from Las Talk 132: Nutrient fluxes in the groundwater affecting Chinas-Cerro Guido Complex, Magallanes Region, the northern mangrove coast of the peninsula Yucatán Southern Chile: A Key Area for the Antarctic-South (México) American Biogeography Lisa Krienen, Thomas Rüde, Eduardo Graniel Castro and Antonio Marcelo Leppe, Wolfgang Stinnesbeck, Eberhard Frey, Héctor Cardona Benavides Mansilla, Manfred Vogt, Edwin Gonzalez, Leslie Manriquez, Katherine Cisternas, Maritza Mihoc and Toshiro Jujihara -
Management Plan for Antarctic Specially Protected Area No 151
Measure 5 (2019) Management Plan for Antarctic Specially Protected Area No 151 Lions Rump, King George Island, South Shetland Islands Introduction Lions Rump (62º08’S; 58º07’W) is located on the southwestern coast of King George Island, South Shetland Islands, covering approximately 1.32 km2 in area. The Area takes its name from the distinctive rocky hill lying between the southern extremity of King George Bay and Lions Cove. The Area was originally designated as Site of Special Scientific Interest No 34 through Recommendation XVI-2 (1991, SSSI No 34) after a proposal by Poland on the grounds that it contains diverse biota and geological features and is a representative example of the terrestrial, limnological, and littoral habitats of the maritime Antarctic. The Area was designated primarily to protect its ecological values. It is also valuable as a reference site with diverse avian and mammalian Antarctic fauna, against which disturbance at sites situated near locations of human activity can be measured. A revised Management Plan was adopted in Measure 1 (2000). The site was re-designated ASPA No 151 in Decision 1 (2002). A second revised Management Plan was adopted in Measure 11 (2013). Based on the Environmental Domains Analysis for Antarctica (Resolution 3 (2008)) ASPA No 151 lies within Environment A (Antarctic Peninsula northern geologic), which is a small, terrestrial environment around the northern Antarctic Peninsula consisting entirely of ice-free land cover and sedimentary geology (Morgan et al. 2007). Other protected areas containing Domain A include ASPA No 111, ASPA No 128 and ASMA No 1 (Morgan et al. -
New Paleomagnetic Pole for the Upper Jurassic Chon
Tectonophysics 750 (2019) 45–55 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto New paleomagnetic pole for the Upper Jurassic Chon Aike Formation of T southern Argentina (South America): Testing the tectonic stability of Patagonia with respect to South America, and implications to Middle Jurassic-Early Cretaceous true polar wander ⁎ Víctor Ruiz Gonzáleza, , Carla G. Puigdomenecha, Emiliano M. Rendaa, Bárbara Boltshausera, Rubén Somozaa, Haroldo Vizána, Claudia B. Zaffaranab, Graeme K. Taylorc, Miguel Hallerd, Raúl Fernándeze a IGEBA, UBA – CONICET, Argentina b IIPG, UNRN – CONICET, Argentina c Plymouth University, United Kingdom d CENPAT, CONICET – UNPSJB, Argentina e INREMI, UNLP, Argentina ARTICLE INFO ABSTRACT Keywords: A paleomagnetic pole and a new Ar-Ar date of 156.08 ± 0.05 Ma are reported for the Chon Aike Formation, an Chon Aike Formation extensive plateau of ignimbrites, outcropping in the Deseado Massif (southern Patagonia, Argentina). The Deseado Massif geographic coordinates and statistical parameters for the paleomagnetic pole, validated by a reversal test, are: South America Lat. = 84.3° S, Long. = 191.3° E, A95 = 8.6°, K = 13.3, N = 23. This pole shows a complete coherence with Late Paleomagnetism Jurassic and Early to mid-Cretaceous poles of South America, obtained exclusively from igneous rocks, avoiding Apparent polar wander path any potential inclination shallowing. It is suggested that; a) southern Patagonia was an integral part of South America in the Late Jurassic; b) any reported vertical axis tectonic rotations must pre-date the Late Jurassic in this region; c) according to updated paleomagnetic data from igneous rocks, South America had very limited latitudinal drift between about 160 and 140 Ma; and, therefore, d) its apparent polar wander (APW) path, when compared with global apparent polar wander paths, does not support a large global shift or true polar wander (TPW) between 160 and 140 Ma. -
Chile: a Journey to the End of the World in Search of Temperate Rainforest Giants
Eliot Barden Kew Diploma Course 53 July 2017 Chile: A Journey to the end of the world in search of Temperate Rainforest Giants Valdivian Rainforest at Alerce Andino Author May 2017 1 Eliot Barden Kew Diploma Course 53 July 2017 Table of Contents 1. Title Page 2. Contents 3. Table of Figures/Introduction 4. Introduction Continued 5. Introduction Continued 6. Aims 7. Aims Continued / Itinerary 8. Itinerary Continued / Objective / the Santiago Metropolitan Park 9. The Santiago Metropolitan Park Continued 10. The Santiago Metropolitan Park Continued 11. Jardín Botánico Chagual / Jardin Botanico Nacional, Viña del Mar 12. Jardin Botanico Nacional Viña del Mar Continued 13. Jardin Botanico Nacional Viña del Mar Continued 14. Jardin Botanico Nacional Viña del Mar Continued / La Campana National Park 15. La Campana National Park Continued / Huilo Huilo Biological Reserve Valdivian Temperate Rainforest 16. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued 17. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued 18. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued / Volcano Osorno 19. Volcano Osorno Continued / Vicente Perez Rosales National Park 20. Vicente Perez Rosales National Park Continued / Alerce Andino National Park 21. Alerce Andino National Park Continued 22. Francisco Coloane Marine Park 23. Francisco Coloane Marine Park Continued 24. Francisco Coloane Marine Park Continued / Outcomes 25. Expenditure / Thank you 2 Eliot Barden Kew Diploma Course 53 July 2017 Table of Figures Figure 1.) Valdivian Temperate Rainforest Alerce Andino [Photograph; Author] May (2017) Figure 2. Map of National parks of Chile Figure 3. Map of Chile Figure 4. Santiago Metropolitan Park [Photograph; Author] May (2017) Figure 5. -
Chapter 4 Tectonic Reconstructions of the Southernmost Andes and the Scotia Sea During the Opening of the Drake Passage
123 Chapter 4 Tectonic reconstructions of the Southernmost Andes and the Scotia Sea during the opening of the Drake Passage Graeme Eagles Alfred Wegener Institute, Helmholtz Centre for Marine and Polar Research, Bre- merhaven, Germany e-mail: [email protected] Abstract Study of the tectonic development of the Scotia Sea region started with basic lithological and structural studies of outcrop geology in Tierra del Fuego and the Antarctic Peninsula. To 19th and early 20th cen- tury geologists, the results of these studies suggested the presence of a submerged orocline running around the margins of the Scotia Sea. Subse- quent increases in detailed knowledge about the fragmentary outcrop ge- ology from islands distributed around the margins of the Scotia Sea, and later their interpretation in light of the plate tectonic paradigm, led to large modifications in the hypothesis such that by the present day the concept of oroclinal bending in the region persists only in vestigial form. Of the early comparative lithostratigraphic work in the region, only the likenesses be- tween Jurassic—Cretaceous basin floor and fill sequences in South Geor- gia and Tierra del Fuego are regarded as strong enough to be useful in plate kinematic reconstruction by permitting the interpretation of those re- gions’ contiguity in mid-Mesozoic times. Marine and satellite geophysical data sets reveal features of the remaining, submerged, 98% of the Scotia 124 Sea region between the outcrops. These data enable a more detailed and quantitative approach to the region’s plate kinematics. In contrast to long- used interpretations of the outcrop geology, these data do not prescribe the proximity of South Georgia to Tierra del Fuego in any past period. -
New Detrital Zircon U/Pb Geochronology of the Cerro Dorotea, Río Turbio, and Río Guillermo Formations, Magallanes Basin
O EOL GIC G A D D A E D C E I H C I L E O S F u n 2 d 6 la serena octubre 2015 ada en 19 Timing and rates of foreland sedimentation: New detrital zircon U/Pb geochronology of the Cerro Dorotea, Río Turbio, and Río Guillermo formations, Magallanes basin Julie C. Fosdick1*, J. Enrique Bostelmann2, Joel Leonard1, Raúl Ugalde3, José Luis Oyarzún4, and Miguel Griffin5 1: Department of Geological Sciences, Indiana University, 1001 Tenth Street, Bloomington, Indiana, 47405, USA. 2: Red Paleontológica U-Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Santiago, Chile. 3: PEDECIBA Geociencias, Facultad de Ciencias, Universidad de la República, Iguá 4225, Montevideo, Uruguay. 4: Parque Geo-paleontológico La Cumbre-Baguales, Ruta 9 km 284, Magallanes, Chile. 5: CONICET—División PaleoZoología Invertebrados, Museo de La Plata. Paseo del Bosque s/n, La Plata, Argentina. * email: [email protected] Abstract. We report new detrital zircon U/Pb signals (timing, tempo, magnitude) of tectonics, climate, geochronology from the Cenozoic Magallanes foreland and eustasy in the stratigraphic record. For instance, basin (near 51 °S) in both Argentina and Chile, that sheds enhanced tectonism in foreland basin settings can cause light on sedimentary provenance and improved timing of crustal load-driven subsidence and basin deepening. sedimentation for the Cerro Dorotea, Río Turbio, and Río Globally, the growth and ablation of continental ice sheets Guillermo formations. Using youngest detrital age regulates sea level and global climate, and precipitation populations to constrain maximum depositional age (MDA), and temperature gradients influence erosion rates, we provide the first radiometric age confirmation of vegetation cover, and the distribution of deformation. -
ABSTRACTS ACTAS IAGOD 2019 31Ene.Pmd
SALTA, ARGENTINA 28-31 AUGUST 2018 15th Quadrennial International Association on the Genesis of Ore Deposits Symposium SPONSORS PLATINUM SPONSORS GOLD SPONSORS SILVER SPONSORS BRONZE SPONSORS COPPER SPONSORS Co-sponsored by SALTA, ARGENTINA 28-31 AUGUST 2018 15th Quadrennial International Association on the Genesis of Ore Deposits Symposium SYMPOSIUM PROCEEDINGS SCIENTIFIC COMMITTEE CHAIR Lira Raúl – (University of Córdoba – CONICET, Argentina) MEMBERS Bineli-Betsi Thierry – (Botswana International University of Science and Technology) Chang Zhaoshan – (Colorado School of Mines, USA) Cherkasov Sergey – (Vernadsky State Geological Museum of Russian Academy of Sciences) Cook Nigel – (University of Adelaide, Australia) Gozalvez Martín – (Geological and Mining Survey of Argentina) Guido Diego – (CONICET/Austral Gold S.A, Argentina) Lentz David – (University of New Brunswick, Economic Geology Chair) López Luis – (National Atomic Energy Commission, Argentina) Mao Jingwen – (Chinese Academy of Geological Sciences/Hebei GEO University, China) Meinert Larry – (Consultant) Pons Josefina – (IIPG – University of Río Negro – University of Comahue – CONICET, Argentina) Rubinstein Nora – (IGEBa–University of Buenos Aires – CONICET) Sanematsu Kenzo – (Geological Survey of Japan, AIST) Schutesky Della Giustina Maria Emilia – (University of Brasília, Brasil) Tornos Fernando – (Spanish National Research Council – CSIC) Watanabe Yasushi – (Faculty of International Resource Sciences, Akita University, Japan) EDITED BY Daniel Rastelli, Dolores Álvarez, Noelia -
List of Place-Names in Antarctica Introduced by Poland in 1978-1990
POLISH POLAR RESEARCH 13 3-4 273-302 1992 List of place-names in Antarctica introduced by Poland in 1978-1990 The place-names listed here in alphabetical order, have been introduced to the areas of King George Island and parts of Nelson Island (West Antarctica), and the surroundings of A. B. Dobrowolski Station at Bunger Hills (East Antarctica) as the result of Polish activities in these regions during the period of 1977-1990. The place-names connected with the activities of the Polish H. Arctowski Station have been* published by Birkenmajer (1980, 1984) and Tokarski (1981). Some of them were used on the Polish maps: 1:50,000 Admiralty Bay and 1:5,000 Lions Rump. The sheet reference is to the maps 1:200,000 scale, British Antarctic Territory, South Shetland Islands, published in 1968: King George Island (sheet W 62 58) and Bridgeman Island (Sheet W 62 56). The place-names connected with the activities of the Polish A. B. Dobrowolski Station have been published by Battke (1985) and used on the map 1:5,000 Antarctic Territory — Bunger Oasis. Agat Point. 6211'30" S, 58'26" W (King George Island) Small basaltic promontory with numerous agates (hence the name), immediately north of Staszek Cove. Admiralty Bay. Sheet W 62 58. Polish name: Przylądek Agat (Birkenmajer, 1980) Ambona. 62"09'30" S, 58°29' W (King George Island) Small rock ledge, 85 m a. s. 1. {ambona, Pol. = pulpit), above Arctowski Station, Admiralty Bay, Sheet W 62 58 (Birkenmajer, 1980). Andrzej Ridge. 62"02' S, 58° 13' W (King George Island) Ridge in Rose Peak massif, Arctowski Mountains. -
Geochemical Characteristics of the Infilling of Ground Wedges at Puerto Deseado (Santa Cruz, Argentina): Palaeoenvironmental and Chronological Implications
Andean Geology ISSN: 0718-7092 ISSN: 0718-7106 [email protected] Servicio Nacional de Geología y Minería Chile Geochemical characteristics of the infilling of ground wedges at Puerto Deseado (Santa Cruz, Argentina): palaeoenvironmental and chronological implications Zanchetta, Giovanni; Ribolini, Adriano; Ferrari, Matteo; Bini, Monica; Isola, Ilaria; Lezzerini, Marco; Baroni, Carlo; Salvatore, Maria Cristina; Pappalardo, Marta; Fucks, Enrique; Boretto, Gabriella Geochemical characteristics of the infilling of ground wedges at Puerto Deseado (Santa Cruz, Argentina): palaeoenvironmental and chronological implications Andean Geology, vol. 45, no. 2, 2018 Servicio Nacional de Geología y Minería, Chile Available in: https://www.redalyc.org/articulo.oa?id=173955659002 DOI: https://doi.org/10.5027/andgeoV45n2-3070 PDF generated from XML JATS4R by Redalyc Project academic non-profit, developed under the open access initiative Andean Geology, 2018, vol. 45, no. 2, ISSN: 0718-7092 0718-7106 Artículos de Investigación Geochemical characteristics of the infilling of ground wedges at Puerto Deseado (Santa Cruz, Argentina): palaeoenvironmental and chronological implications Características geoquímicas de las cuñas de hielo en Puerto Deseado (Santa Cruz, Argentina): implicancias paleoambientales y cronológicas Giovanni Zanchetta DOI: https://doi.org/10.5027/andgeoV45n2-3070 Istituto Nazionale Geofisica e Vulcanologia Roma, Italia Redalyc: https://www.redalyc.org/articulo.oa? [email protected] id=173955659002 Adriano Ribolini University -
a Pleistocene Ice Sheet in the .' Northern Boulder Mountains
, A Pleistocene Ice Sheet in the .' Northern Boulder Mountains .< Jefferson, Powell, and Lewis and Clark Counties, Montana By EDWARD T. RUPPEL CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1141-G A descriptive report of the glacial geology in the northern part of the Boulder Mountains, Montana UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract- _______-_-______-__-_--____--___________--____-_-_-______ G-1 Introduction. _ _____________________________________________________ 1 Summary of bedrock geology.___-___-____.____._-___._.__--__--_.___ 4 Surficial geology.._________________________________________________ 5 Northern Boulder Mountains ice sheet- ___-____-___.----_-_--_-__ 5 Glacial erosion.___________________________________________ 7 Glacial deposits.-______--_^______-________________________ 9 Age and regional relations of glaciation.___:______.____________ 11 Postglacial erosion.---___-_--________-___---___-_-------__---__ 13 Creep-and-solifluction deposits and stone-banked terrace deposits. 14 Frost-wedged rock waste and boulders of disintegration........ 15 Landslides._______________________________________________ 19 Bog and swamp deposits. _______________________________"___ 20 Age of mass-wasting deposits--....----...--___---__---_--_. 20 References cited..____________________________ _____________________ 21 ILLUSTRATIONS [Plates in pocket] PLATE 1. Ice coverage and flow, Basin quadrangle, Jefferson, Lewis and Clark, and Powell Counties, Mont. 2. Interpretations of Pleistocene and Recent history, Montana and adjacent areas. FIGURE 1. Inferred limits of northern Boulder Mountains ice sheet, G-2 2. Typical rounded topography along Continental Divide in northern part of Boulder Mountains---.-,-.------ ------- 3 3. -
West Antarctica: Tectonics and Paleogeography
Chapter 2 West Antarctica: Tectonics and Paleogeography The origin of West Antarctica (WANT) can be traced back to the Terra Australis orogenesis that began between 520 Ma and 510 Ma—shortly after the terminal suturing of Gondwana (Boger 2011). The onset of this event was responsible for the termination of passive margin sedimentation along much of the Pacific margin of Gondwana and marks the beginning of widespread and broadly coeval deforma- tion and arc-type plutonism. It also began a long-lived process of accretion that added much of the crust that defines eastern Australia, West Antarctica (domain 5 of Boger 2011, Fig. 2.1), and western South America (Cawood 2005, 2009). Post-Gondwana accretionary growth—the Terra Australis and Gondwanide Orogenies—The suturing of the West Gondwana and Australo–Antarctic plates along the Kuunga Orogen brought to an end the long-lived process of convergence between the pre-collision components of Gondwana. The result was a reconfigura- tion of the early to middle Cambrian plate system and the consequent transfer of ocean floor consumption from between the pre-Gondwana cratons to the outboard Pacific margin of newly formed Gondwana supercontinent (Cawood2005 ). This led to the establishment of the accretionary Terra Austrais Orogen (Cawood 2005), a general name given to the orogenic belt that stretched continuously from north- ern South America to northern Australia and which began in the early to middle Cambrian and lasted until the late Carboniferous. In Antarctica Terra Australis (Ross) orogenesis also deformed and variably metamorphosed the pre-Gondwana passive margin (Fig. 2.2). The Gondwana supercontinent underwent a sequential fragmentation over approximately 165 Ma. -
ARC Centre of Excellence in Ore Deposits
Università degli Studi di Padova University of Tasmania DIPARTIMENTO DI GEOSCIENZE CODES - ARC Centre of Excellence in Ore Deposits ________________________________________________________________ SCUOLA DI DOTTORATO DI RICERCA IN: SCIENZE DELLA TERRA CICLO XXVI Jurassic magmatism in Patagonia, Mauritania and Mali: Examples of silicic and basaltic Large Igneous Provinces Direttore della Scuola: Ch.mo Prof. Massimiliano Zattin Supervisore: Ch.mo Prof. Andrea Marzoli Co-supervisore: Ch.mo Prof. Vadim Kamenetsky Dottorando: Lina Maria Serrano Duran ABSTRACT At the end of the Triassic and during Jurassic times, the Central Atlantic Magmatic Province (CAMP) with a dominant mafic composition, and the mainly felsic Patagonian Province (PA) were formed in the context of Pangea break-up. CAMP basaltic to basaltic-andesitic dykes and sills from Hank and Hodh, in Mauritania, and Kaarta, in Mali, were emplaced at ca. 197 Ma yielding a signature defined by low to high TiO2-values (0.39 - 2.29 wt.%), Nb-Ta troughs, Pb spikes and enriched Nd-Sr-Pb 143 144 87 86 207 204 compositions ( Nd/ Nd201Ma: 0.51224 - 0.51241, Sr/ Sr201Ma: 0.70572 - 0.70795, Pb/ Pb201Ma: 208 204 206 204 15.61 – 15.68 Pb/ Pb201Ma: 38.44 – 38.07 and Pb/ Pb201Ma: 18.11 – 18.48). Nb/U ratios (= 12 – 15), tracers of recycled material, combined with enriched isotopic signatures suggest the contribution of continental crust in the origin of these magmas. Differences in the ratios of La/Yb of the whole set suggest the existence of an enriched group in Kaarta (La/YbN>4.3) coupled to increasing ratios of Nb/Zr and Th/Y, probably reflecting lower degrees of partial melting in these rocks.